| 红旗岭岩浆硫化铜镍矿床地质特征 |
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| 引用本文： | 秦宽.红旗岭岩浆硫化铜镍矿床地质特征[J].吉林地质,1995,14(3):17-30. |
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| 作者姓名： | 秦宽 |
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| 作者单位： | 吉林镍业公司 |
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| 基金项目： | 1990～1992年《红旗岭铜镍矿区地质背景成岩（矿）规律和找矿方向》合作项目 |
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| 摘 要： | 本文综述了呼兰群地层总体为下古生界，其中黄莺屯组（下段为矿床围岩）相当于寒武－奥陶系，小三个顶子组（为第Ⅲ岩带围岩）属志留一泥盆系；辉发河深断裂为导岩（矿）构造，北西向断裂为容岩（矿）构造。系统地探讨了红旗岭岩浆硫化铜镍矿床（１号、７）号成岩（矿）的地质特征，重新划分了矿床的成因类型。
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| 关 键 词： | 岩浆 岩体 镍矿床 铜矿床 地质特征 |
GEOLOGICAL FEATURES OF MAGMATIC SULFIDE Cu-Ni DEPOSIT AT THE HONGQILING,JILIN PROVINCE |
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| Qin Kuan.GEOLOGICAL FEATURES OF MAGMATIC SULFIDE Cu-Ni DEPOSIT AT THE HONGQILING,JILIN PROVINCE[J].Jilin Geology,1995,14(3):17-30. |
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| Authors: | Qin Kuan |
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| Abstract: | Most of the Hulan group strata belong to an early Paleozoic Era,among them,theHuangyintun Formation is equivalent to the Cambrian-Ordovician,(Lower is a cotintryrocks). Xiaosandingzi Formation belongs to Silurian-Devonian system(Country rock of thethird rock belt),Huifahe deep faults are structures as passage ways for rock(ore)fluids, NWfaults are structures for rock(ore)housing.Metallogenic characteristics of the Hongqilingmagmatic sulfide copper-nickel deposits(No.1, No. 7)are systematically discussed,therefore,the genetic types of deposits are subdivided. |
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| Keywords: | Hongqiling Rockbody No 1 Rockbody No 7 Geological featuresCopper-nickel deposit Genetic type of deposit |
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